Zygopterid ferns †
Important ferns of the Mississippian-Permian
The zygopterids were an important component of the flora from the Mississippian into the Permian. Many features indicate adaptations to growing in dry conditions and high light levels (e.g. strong pubescence; presence of protected shoot tips, which show a periodic dormancy)
Ecology & Form
Stem
Stems that were mostly herbaceous with small amounts of wood (secondary growth)
Most plants were small, but some reached 3 m in height
Main axis is protostele (radial)
Secondary growth comes from a unifacial (one-sided) cambium, unlike woody (lignophyte) plants
Only wood (secondary xylem) produced; not secondary phloem [this is analogous to the unifacial cambium of the lepidodendrids)
Secondary growth only in periclinal divisions (adding girth)
No anticlinal division observed which would add more cambial initials as stem increases in girth
Periderm has been observed in the rhizome of Zygopteris (Scott 1912; Phillips and Galtier 2005)
Leaf
Morphology
The rachis is radially symmetrical in x.s., unlike the bilaterally symmetrical arrangement in true ferns
Referred to as a phyllophore (Phillips 1974)
Etapteroid type: three-dimensional fronds that were quadriserate (=pinna in four ranks or rows); open peripheral loops
Clepsydroid type: two-ranks of primary pinna, similar to modern ferns, with an hour-glass, H-shaped (clepsydroid) anatomy; closed peripheral loops
The pinnae are small and planated
Ultimate pinnae have dichotomizing veins.
Anatomy
Rachis trace can be C-, E-, H-, I-, X, or Y-shaped
Phyllophore exhibits bipolar primary strands, sometimes with peripheral loops
Reproduction
Fertile fronds have clusters of sporangia that replace pinnules
Sporangia are elongate and produced in large clusters on abaxial surface
Classification
└Zygopteridales †
Geologic Age
Late Devonian (Frasnian) - Early Cretaceous (?Cenomanian)
Above: Diagram showing quadriseriate branching, creating four rows along the main axis
Above: Hourglass-shaped anatomy with peripheral loops (PL) in cross-section of Clepsydropsis (Etapteris) leclercqii (Fig. 13, Smoot & Taylor 1978)
Diversity
Alloiopteris †
Potonié 1897
A. arkansana; A. plumosaeformis; A. winslovi
Asterochlaena †
Corda 1845
Permian
Stem, 8cm in width, with deeply-lobed primary xylem and shoot-born roots and phyllophores with clepsydroid anatomy
Leaf traces arise from the lobes to become hourglass-shaped
Asterochlaenopsis kirgisica †
Sahni 1930
Permian of Siberia
Stem with cylindrical stele and a mixed pith
Austroclepsis australis †
Sahni 1932
Tournaisian of Australia
Tree fern with 30 cm wide "false stem" with numerous stems with leaves and roots
Biscalitheca †
Mamay 1957
B. kansana; B. musata; B. suzanneana
Brittsia †
Clepsydropsis †
Unger 1856
Small, C-shaped pinna traces and peripheral loops with little parenchyma (Phillips & Galtier 2005)
C. bertrandi; C. campbelli; C. chaneyi; C. leclercqii; C. titan
Corynepteris †
Dernbachia brasiliensis †
Rössler & Galtier 2002
Permian of Brazil
Small tree fern with 6-18 cm in diameter with large actinostele surrounded by a narrow cortex extending into leaf bases and root mantle
Leaf traces depart stele as oval traces and become π-shaped; leaves arrange in pseudowhorls
Diplolabis †
Ellesmeris †
Early Late Devonian (Frasnian) of southern Ellesmere Island, Canadian Arctic Archipelago.
Plant occurs in an Archaeopteris-dominated flora preserved in the Nordstrand Point Formation (Mid-Late Frasnian) near Bird Fjord.
The plant has a pinnate vegetative system with three branch orders and laminate sphenopteroid pinnules.
Primary pinnae usually diverge from the main axis in distichous pairs (quadriseriate), but can depart singly (biseriate).
Each primary pinna bears a basal catadromic aphlebia.
Anatomically, the plant exhibits a mesarch bipolar protostele that is ribbon- to clepsydropsoid-shaped in the main axis.
Primary pinna traces are also initially bipolar and crescent-shaped, but may become four-ribbed before dividing into a pair of bipolar traces.